摘要
武夷山成矿带是我国重点成矿带之一,分布着众多的铜铅锌银等多金属矿床,矿床类型多样。本文在讨论陈坊铜多金属矿成矿地质特征的基础上,通过系统研究陈坊地区石炭纪地层中受接触带构造控制的矽卡岩型和二叠纪地层中主要为受层间破碎带控制的矽卡岩型铜铅锌多金属矿体的分布特征,探讨该区控矿因素、矿床成因分析,表明陈坊矿区成矿潜力巨大,并提出该区下一步找矿方向的建议。
The Wuyishan mountain metallogenetic belt is one of the important metallogenetic belts in China,where are distributed amounts of copper,lead, zinc and silver polymetallic deposits of multiple type. Based on analysing metallogenetic geological characteristics of the Chenfang copper-polymetallic deposit, this paper systematically studies the distribution features of skarn-type copper,lead and trolling factors and geneses of deposits. The result of the study indicates the great metallogenetic potentials of the Chenfang mineralizing area,therefore the ore-prospecting direction of the area in the next stage is suggested.
出处
《资源调查与环境》
2008年第4期279-288,共10页
Resources Survey & Environment
基金
中国地质调查局"江西怀玉山-北武夷铜多金属矿评价"项目(1212010532901)资助
关键词
矽卡岩型
铜多金属矿
找矿方向
北武夷
陈坊
skarn-type
eopper-polymetallic ore deposit
ore-prospecting direction
northern Wuyishan mountain area
Chenfang area